C23A:
Frozen Soil, Its Change, and the Responses and Feedbacks of the Frozen Soil Change in Atmosphere, Hydrology, and Ecosystem II Posters


Session ID#: 8437

Session Description:
Frozen soil is an important component of cryosphere. Atmosphere, frozen soil, water and ecosystem together form a dynamic system that is filled with responses and feedbacks. Distinctive features in atmosphere, hydrology and ecosystems are associated with the frozen soil. For example, at different thawing and freezing stages, soil surface sensible and latent heat fluxes assume dominant roles differently. Permafrost soil limits the interaction between soil surface and deep groundwater due to the hydraulic impedance. In high altitudes, the wetland ecosystem is associated with the permafrost soil. With warming climate, frozen soil degradation has been reported in the high latitudes and altitudes. Components of the dynamic system are expected to alter, and so do the responses and feedbacks among the components. In this session, we welcome studies that focus on the frozen soil modeling and observation, the mechanisms of frozen soil change, and the responses and feedbacks in the dynamic system.
Primary Convener:  Lan Cuo, ITP Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing, China
Conveners:  Yanhong Gao, Northwest Institute of Eco-Environment and Resources, CAS, Lanzhou, China, Shilong Piao, Peking University, College of Urban and Environmental Sciences, Beijing, China and Lin Zhao, LZU Lanzhou University, Lanzhou, China
Chairs:  Lan Cuo, ITP Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing, China and Lin Zhao, LZU Lanzhou University, Lanzhou, China
OSPA Liaison:  Yanhong Gao, Northwest Institute of Eco-Environment and Resources, CAS, Lanzhou, China

Cross-Listed:
  • A - Atmospheric Sciences
  • B - Biogeosciences
  • GC - Global Environmental Change
  • H - Hydrology
Index Terms:

0702 Permafrost [CRYOSPHERE]
0704 Seasonally frozen ground [CRYOSPHERE]
1621 Cryospheric change [GLOBAL CHANGE]
1807 Climate impacts [HYDROLOGY]

Abstracts Submitted to this Session:

Seasonal Variation of Arsenic Concentrations in Natural Water of the Source Area of the Yellow River on the Qinghai-Tibet Plateau, China (86375)
Congrong Yu, Hohai University, Nanjing, China
IMPACT OF CRITICAL ANION SOIL SOLUTION CONCENTRATION ON ALUMINUM ACTIVITY IN ALPINE TUNDRA SOIL Andrew Evans, Jr.1 , Michael B. Jacobs2, and Jason R. Janke1, (1) Metropolitan State University of Denver, Dept. of Earth and Atmospheric Sciences, (2) Dept. of Chemistry, Denver, CO, United States. (86503)
Andrew Evans, Metropolitan State University of Denver, Denver, CO, United States
Controls on Snowmelt Partitioning to Surface and Groundwater Flow (59175)
Alice Frances Hill, National Institute of Water and Atmospheric Research (NIWA), Nelson, New Zealand, Mark W Williams, Univ Colorado, Boulder, CO, United States and Kurt Chowanski, Institute for Arctic and Alpine Research, Boulder, CO, United States; South Dakota State University, Department of Natural Resource Management, Rapid City, SD, United States
Wind erosion simulation along with the Qinghai-Tibet Railway and its response to the climate change (64061)
Yingsha Jiang, Northwest Institue of Eco-Environment and Resources, CAS, Lanzhou, China and Yanhong Gao, Northwest Institute of Eco-Environment and Resources, CAS, Lanzhou, China
Aridity changes over the Tibetan Plateau in recent three decades (64114)
Xia Li, CAREERI/CAS Cold and Arid Regions Environmental and Engineering Research Institute, Lanzhou, China and Yanhong Gao, Northwest Institute of Eco-Environment and Resources, CAS, Lanzhou, China
The Plant Foliage Projective Coverage Change over the Northern Tibetan Plateau during 1957-2009 (76196)
Lan Cuo, ITP Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing, China
Soil temperature change on the Tibetan Plateau (79624)
Fuxin Zhu1, Lan Cuo1, Yongxin Zhang2 and Jing-Jia Luo3, (1)ITP Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing, China, (2)National Center for Atmospheric Research, Boulder, United States, (3)Bureau of Meteorology, Melbourne, Australia
Hillslope-scale variability in seasonal frost depth and soil water content investigated by GPR on the southern margin of the sporadic permafrost zone on the Tibetan Plateau (75174)
Sebastian Zubrzycki, University of Hamburg, Hamburg, Germany, Yingzhao Ma, ITP Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing, China and Yinsheng Zhang, Key Laboratory of Tibetan Environment Changes and Land Surface Processes, Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing, China
Development of An Enthalpy-based Frozen Soil Model and Its Validation in A Cold Region in China (66047)
Huiyi Bao, University of Tokyo, Bunkyo-ku, Japan
Augmentation of freeze-thaw cycles in the alpine soil triggered by the fire on the alpine slopes, Mount Shirouma-dake, northern Japanese Alps (72126)
Akihiko Sasaki, Kokushikan University, Setagaya, Tokyo, Japan and Keisuke Suzuki, Shinshu University, Matsumoto, Japan
Impacts of Short-Term Meteorological Fluctuations on Near-Surface Ground Temperatures in Spitsbergen, Svalbard (83514)
Sarah Marie Strand and Hanne H. Christiansen, University Centre in Svalbard, Arctic Geology Department, Longyearbyen, Norway

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